4.3 Article

Transmission electron microscopy study of aerosol particles from the brown hazes in northern China

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AMER GEOPHYSICAL UNION
DOI: 10.1029/2008JD011285

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  1. National Basic Research Program of China [2006CB403701]
  2. Cultivation Fund of the Key Scientific and Technical Innovation Project of the Ministry of Education of China [705022]
  3. National Science Foundation of China [40575065]

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Airborne aerosol collections were performed in urban areas of Beijing that were affected by regional brown haze episodes over northern China from 31 May to 12 June 2007. Morphologies, elemental compositions, and mixing states of 810 individual aerosol particles of different sizes were obtained by transmission electron microscopy coupled with energy-dispersive X-ray spectrometry. The phases of some particles were verified using selected-area electron diffraction. Aerosol particle types less than 10 mm in diameter include mineral, complex secondary (Ca-S, K-, and S-rich), organic, soot, fly ash, and metal (Fe-rich and Zn-bearing). Most soot, fly ash, and organic particles are less than 2 mu m in diameter. Approximately 84% of the analyzed mineral particles have diameters between 2 and 10 mu m, while 81% of the analyzed complex secondary and metal particles are much smaller, from 0.1 to 2 mu m. Trajectory analysis with fire maps show that southerly air masses arriving at Beijing have been transported through many agricultural biomass burning sites and heavy industrial areas. Spherical fly ash and Fe-rich particles were from industrial emissions, and abundant K- rich and organic particles likely originated from field burning of crop residues. Abundant Zn-bearing particles are associated with industrial activities and local waste incinerators. On the basis of the detailed analysis of 443 analyzed aerosol particles, about 70% of these particles are internally mixed with two or more aerosol components from different sources. Most mineral particles are covered with visible coatings that contain N, O, Ca (or Mg), minor S, and Cl. K- and S-rich particles tend to be coagulated with fly ash, soot, metal, and fine-grained mineral particles. Organic materials internally mixed with K- and S-rich particles can be their inclusions and coatings.

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